Palaeohydrological changes in the upper Dneper Valley, Belarus, during the last 20 000 years
Palaeohydrology and environmental change
the Subatlantic about 2100 and 1000 BP manifested themselves here by changes of the type of sedimentation on flood plains (buried soils). These phases are conditioned by the climate, altough in the younger one a remarkable influence of human activity is evident
To provide characteristics of present-day extreme events which may serve as a key to better recognition of past hydrological changes, the upper Vistula basin was taken as an example. The observations are mainly related to last 100-150 years